Letters

EARLY SCIENCE WITH SOFIA, THE STRATOSPHERIC OBSERVATORY FOR INFRARED ASTRONOMY

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Published 2012 March 29 © 2012. The American Astronomical Society. All rights reserved.
, , Citation E. T. Young et al 2012 ApJL 749 L17 DOI 10.1088/2041-8205/749/2/L17

2041-8205/749/2/L17

ABSTRACT

The Stratospheric Observatory For Infrared Astronomy (SOFIA) is an airborne observatory consisting of a specially modified Boeing 747SP with a 2.7 m telescope, flying at altitudes as high as 13.7 km (45,000 ft). Designed to observe at wavelengths from 0.3 μm to 1.6 mm, SOFIA operates above 99.8% of the water vapor that obscures much of the infrared and submillimeter. SOFIA has seven science instruments under development, including an occultation photometer, near-, mid-, and far-infrared cameras, infrared spectrometers, and heterodyne receivers. SOFIA, a joint project between NASA and the German Aerospace Center Deutsches Zentrum für Luft und-Raumfahrt, began initial science flights in 2010 December, and has conducted 30 science flights in the subsequent year. During this early science period three instruments have flown: the mid-infrared camera FORCAST, the heterodyne spectrometer GREAT, and the occultation photometer HIPO. This Letter provides an overview of the observatory and its early performance.

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1. INTRODUCTION

The Stratospheric Observatory For Infrared Astronomy (SOFIA) is a joint project of the National Aeronautics and Space Administration, USA (NASA) and the German Aerospace Center Deutsches Zentrum für Luft und-Raumfahrt (DLR). The NASA and DLR development and operations costs, as well as the science observing time, are divided up in 80:20 proportions, respectively. SOFIA consists of a 2.7 m telescope developed by DLR that resides in a highly modified Boeing 747SP aircraft, enabling observations of a wide variety of astronomical objects at wavelengths from 0.3 μm to 1.6 mm (Stutzki 2006; Becklin et al. 2007; Gehrz et al. 2009). The SOFIA telescope design and its evolving instrument complement build upon the legacy of NASA's Kuiper Airborne Observatory (KAO), a 0.9 m infrared telescope that flew from 1974 to 1995 in a Lockheed C141 Starlifter aircraft (Gillespie 1981). SOFIA flies at altitudes of up to 13.7 km (45,000 ft), which is above 99.8% of the atmospheric water (H2O) vapor. At SOFIA's operational altitudes, the typical precipitable H2O column depth is about 10 μm (roughly a hundred times lower than at good terrestrial sites). This enables observations in large parts of the infrared spectrum that are inaccessible from the ground. Figure 1 compares the computed atmospheric transmission from the operating altitude of SOFIA with that from one of the best terrestrial sites, the 5612 m Cerro Chajnantor site in Chile. The calculations were done using the ATRAN model (Lord 1992) and assume a median precipitable water vapor of 0.7 mm for Cerro Chajnantor (Radford et al. 2008). In addition to providing access to virtually all of the infrared, SOFIA, with its projected 20 year operational lifetime, serves as a platform for the development of new generations of instruments. Education and public outreach are important elements of the SOFIA mission. Consequently, the design of SOFIA included from the beginning provisions for flying educators who would be able to share the scientific experience with students.

Figure 1.

Figure 1. Calculated atmospheric transmission for SOFIA and Cerro Chajnantor. Computed using the ATRAN program (Lord 1992) assuming 10 μm and 700 μm of precipitable water vapor, respectively. The average SOFIA transmission between 20 μm and 1.3 mm is 80%.

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A schematic view of the SOFIA facility is shown in Figure 2. The telescope resides in an open cavity in the aft section of the aircraft and views the sky through a port-side doorway. The door has a rigid upper segment and a flexible lower segment that can be tracked together to allow the telescope to operate, unvignetted, over an elevation range of 23°–58°. The telescope is moved by magnetic torquers around a 1.2 m diameter spherical hydrostatic bearing that floats under an oil pressure of 20 atmospheres within two closely fitting spherical rings. The rings are mounted in the 6.4 m diameter pressure bulkhead on the axis of the Nasmyth beam. The travel of the bearing for azimuth tracking is only ±3°  so the aircraft heading must be periodically adjusted to keep the source within the telescope field of view (FOV). The forward part of the airplane is pressurized, and the working environment for the crew is typical of that in a commercial airliner. This pressurized region provides access to the science instrument during the flight. The characteristics of the SOFIA observatory are given in Table 1.

Figure 2.

Figure 2. Cutaway schematic of the SOFIA observatory. The pressurized cabin is to the left of the pressure bulkhead. The telescope looks out from the port side of the airplane. The 10,000 kg mass is supported by a hydrostatic spherical bearing that allows an elevation range of 23°–58°. The light for the science instrument is fed through the Nasmyth tube which goes through the bearing. An environmental control system prevents condensation during descent when the door is closed after a night of observations.

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Table 1. SOFIA Observatory Characteristics

Characteristic Value
Operational wavelength 0.3–1600 μm
Clear aperture diameter 2.5 m
Telescope elevation range (unvignetted) 23°–58°
Unvignetted FOV 8'
Telescope optics image quality at 0.6 μma 1farcs6 (80% encircled energy)
Diffraction-limited image size (FWHM)b 0.0825 × λ(μm) ('')
Chopper frequencies (2 pt square wave) 1–20 Hz
Maximum chop throw (unvignetted) ±5'
Maximum flight altitude 13.7 km (45,000 ft)
Typical flight duration 10 hr
Flight time above 12.5 km (41,000 ft) 6 hr
Operational lifetime 20 yr

Notes. aDoes not include the effects of seeing or pointing stability, which dominate at the shorter wavelengths. bThe goal at full operational capability is diffraction-limited imaging for λ > 15 μm.

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The first SOFIA science observations were conducted in 2010 December using the FORCAST (Faint Object Infrared Camera for the SOFIA Telescope) mid-infrared camera. In the 11 months following this first flight, SOFIA conducted 30 science flights using the FORCAST camera, the GREAT (German Receiver for Astronomy at Terahertz frequencies) heterodyne submillimeter spectrometer, and the HIPO (High-speed Imaging Photometer for Occultations) occultation photometer. This initial phase is known collectively as Early Science and represents a demonstration of initial SOFIA capabilities while the facility and its instrumentation are still under development.

In this Letter, we provide an overview of the telescope and observatory and describe its performance during the Early Science period. We set the context for the rest of the articles in this special issue, which present Early Science results based on observations using the FORCAST mid-infrared instrument during the first three flights. An additional 10 flights with FORCAST were conducted for the general astronomical community, a period called Basic Science. Those results will be described elsewhere. Observations with HIPO during the Early Science period included an occultation of a star by Pluto on 2011 June 23, during which the observatory was flown through the central chord of the shadow cast by Pluto (Person et al. 2011). The GREAT instrument was flown on 16 scientific flights during Early Science. The first results from those observations will appear in parallel in a special issue of Astronomy and Astrophysics.

2. SOFIA TELESCOPE AND OBSERVATORY OVERVIEW

The SOFIA telescope, supplied by DLR as part of the German contribution to SOFIA, is a bent classical Cassegrain with a 2.690 m diameter parabolic primary mirror, and a 0.352 m hyperbolic secondary mirror. The secondary mirror is deliberately undersized and illuminates a 2.5 m diameter effective aperture to enable chopping without spilling the beam onto the warm region surrounding the primary mirror. The secondary mirror is attached to a chopping mechanism providing amplitudes of ±4' at chop frequencies up to 20 Hz. The unvignetted FOV is 8'. The f/19.6 Nasmyth infrared focus is fed by a 45° gold-coated dichroic mirror (Figure 3). This dichroic mirror separates the light into a reflected infrared beam that is sent to the science instrument and a visible light beam that is sent to a CCD guide camera, the Focal Plane Imager (FPI). Two other imaging/guiding cameras, the Wide Field Imager (WFI) and the Fine Field Imager (FFI), are used as part of the acquisition system. They are attached to the front ring of the telescope. Table 2 gives some of the key optical parameters of the SOFIA telescope and guide cameras. A more detailed description of the telescope has been given by Krabbe (2000).

Figure 3.

Figure 3. Schematic of the optical system of the SOFIA telescope (left) and a model of the SOFIA telescope assembly (right). Everything left of the bulkhead is contained in the forward pressurized crew cabin, while everything to the right is contained in the open telescope cavity.

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Table 2. SOFIA Telescope Parameters

Parameter Value
Optical configuration Classical Bent Cassegrain
Primary mirror diameter 2.69 m
Primary mirror material Zerodur
Primary conic constant −1
Primary focal length 3200 mm
Secondary mirror diameter 352 mm
Secondary mirror material Silicon carbide
Secondary radius of curvature 954.13 mm
Secondary conic constant −1.2980
Effective entrance pupil diameter 2.5 m
Nominal focal length 49141 mm
Nominal system f-ratio f/19.6
Wide Field Imager FOV ×
Fine Field Imager FOV 70' × 70'
Focal Plane Imager FOV 8' × 8'

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The pointing of the telescope is performed more like a space telescope than a ground-based telescope. The primary reference frame for SOFIA is a set of fiber optic gyroscopes that maintain an inertial reference frame. Once a target is acquired on the sky, its position is stabilized by these gyroscopes with occasional updates by the guide cameras.

The telescope optics are designed to provide 1farcs1 FWHM images on-axis at 0.6 μm with diffraction-limited performance at wavelengths longer than 15 μm. However, the telescope is subject to various vibrations as well as variable wind loads in flight, which affect the telescope pointing stability and hence the delivered image quality. SOFIA has active and passive damping systems designed to mitigate some of these effects. In the Early Science flights, after limited tuning of the damping systems, the telescope produced an image quality of 3farcs2 FWHM at 19.7 μm with an rms pointing stability of 1farcs7. While these values are large enough to affect image quality at the shorter wavelength end of the SOFIA 0.3–1600 μm observing range, the observatory was nearly diffraction limited at λ > 38 μm (i.e., over the large majority of the SOFIA operating wavelength range) just after First Light.

One of the larger causes of variable image quality is high-velocity turbulent airflow across the cavity, which drives vibrations and leads to elongation of images in the cross-elevation direction. Early tests showed that the magnitude of this effect might also depend on the telescope elevation. Therefore, because of variables like the amount of turbulence and cross-elevation vibration, the point-spread function (PSF) was not stable in the mid-infrared for Early Science from observation to observation.

Further mitigation of the rms pointing jitter through tuning of active control systems and the addition of active mass dampers were implemented in late 2011. These dampers are installed at various locations on the primary and secondary mirror support structures. In the future, after optimization of the damping systems, the rms pointing stability is expected to improve to 0farcs5, which will deliver an image quality of 2farcs1 FWHM at 19.7 μm.

At wavelengths shorter than 10 μm, another significant contributor to the PSF width is the seeing due to turbulence in the shear layer in the vicinity of the airplane. The shear layer seeing is wavelength dependent and increases at shorter wavelengths. Below roughly 5 μm, the shear layer seeing becomes the dominant image size contributor.

The secondary mirror is capable of chopping in any direction from center with a maximum amplitude of 292'', with the additional constraint of a maximum total chop amplitude of 480''. As is the case for all Cassegrain systems, tilting the secondary mirror produces coma. For the SOFIA telescope, the coma causes PSF smearing in the direction of the chop by 2'' per 1' of chop amplitude.

3. SOFIA INSTRUMENTATION

One of the strengths of the SOFIA observatory is the ability to change instruments. Seven first-generation instruments have been developed or are being developed for SOFIA. Collectively, they span a large wavelength range (0.3–250 μm) and include imagers and spectrographs. SOFIA provides several classes of instruments. Facility class instruments are general purpose instruments that are maintained and operated by the observatory. Principal Investigator class instruments are maintained and supported by the instrument teams. Special purpose instruments are specialized capabilities also supported by the instrument teams.

FORCAST (PI: Terry Herter, Cornell University) is a mid-infrared camera operating between 5 and 40 μm. The instrument is described in the following paper by Herter et al. (2012). GREAT (PI: Rolf Güsten, MPIfR; Heyminck et al. 2012) is a heterodyne spectrometer currently operating in the 1.2–2.5 THz frequency range. These instruments were used during Early Science for both guaranteed time observations planned by the instrument teams and for programs from the astronomical community competed via open proposal calls.

Two other instruments, HIPO (PI: Edward Dunham, Lowell Observatory; Dunham et al. 2004) and FLITECAM (First Light Infrared Test Experiment Camera; PI: Ian McLean, UCLA; McLean et al. 2006), were used on development flights on SOFIA. HIPO consists of a pair of high-speed CCD detectors specifically configured to be used for occultation and other high-speed imaging applications. FLITECAM is a near-infrared camera operating between 1 and 5 μm. The instrument also has grisms installed that provide moderate resolution spectroscopy at these wavelengths. All four instruments will be offered to the astronomy community for the first annual observing cycle (Cycle 1).

The remaining three instruments, EXES (Echelon-Cross-Echelle Spectrograph; PI: Matt Richter, UC Davis; Richter et al. 2003), FIFI-LS (Field Imaging Far-infrared Line Spectrometer; PI: Alfred Krabbe, University of Stuttgart; Klein et al. 2010), and HAWC (High-resolution Airborne Wideband Camera; PI: Doyal Harper, U. Chicago; Harper et al. 2004), are expected to be offered in a second annual Call for Proposals (Cycle 2). Table 3 summarizes the characteristics of the First Generation SOFIA Instruments. The SOFIA program also plans to introduce new instruments in future years.

Table 3. SOFIA First Generation Instruments

Name Description PI Institution Wavelengths Spectral
        (μm) Resolution
FORCAST Mid-infrared Camera and Grism Spectrometer T. Herter Cornell 5–40 200
GREAT Heterodyne Spectrometer R. Güsten MPIfR 60–240 106–108
FLITECAM Near-infrared Camera and Grism Spectrometer I. McLean UCLA 1–5 2000
HIPO CCD Occultation Photometer T. Dunham Lowell Obs 0.3–1.1  
EXES Mid-infrared Spectrometer M. Richter UC Davis 5–28 3000, 104, 105
HAWC Far-infrared Camera D. A. Harper U Chicago 50–240  
FIFI-LS Integral Field Far-infrared Spectrometer A. Krabbe U Stuttgart 42–210 1000–3750

Note. aDetails available at http://www.sofia.usra.edu/Science/instruments

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4. SOFIA OPERATIONS

SOFIA is based at the NASA Dryden Aircraft Operations Facility (DAOF) in Palmdale, California. The DAOF is a multi-user NASA facility that supports a number of scientific aircraft. The SOFIA Operations Center (SOC) is located at the DAOF and performs the mission operations and laboratory support for the observatory. The SOFIA Science Center (SSC) is located at the NASA Ames Research Center in Moffett Field, California. Collectively, the SSC and the SOC combine to make up SOFIA Science Mission Operations (SMO), which is responsible for the conduct of the science on SOFIA. The overall SOFIA mission development and operations are managed by NASA's SOFIA Program Office, currently located at the DAOF. The SOFIA aircraft operations are managed by NASA's Dryden Flight Research Center (DFRC), which provides the aircraft maintenance staff, aircraft safety personnel, the pilots, navigators, and other aircraft flight crew members. The SMO is jointly managed by the Universities Space Research Association (USRA) for NASA and by the Deutsches SOFIA Institut (DSI), in Stuttgart, Germany for DLR. Science support for the user community will be provided by the SMO and the DSI.

Typical crew members during the Early Science period consisted of the flight deck (pilot, co-pilot, navigator, and flight engineer), mission operations (mission director, science flight planner, telescope operators), instrument team, engineering support (safety technicians, telescope engineers, and water vapor monitor engineer), and General Investigators (GIs).

SOFIA will mainly operate from its home base at DAOF but will also be deployed to operate from other bases in various parts of the world. In particular, regular deployments to the Southern Hemisphere are planned to provide access to targets that cannot be observed from the Palmdale base.

To maximize the operational efficiency of SOFIA, observations are all queue scheduled. Starting in Cycle 1, the bulk of SOFIA observing time will be awarded on a yearly basis via open, peer-reviewed proposal calls, and observations will be awarded in units of time. Thus, there will be a process of flight planning for every observing cycle which will be very much like planning year-long observations for a space mission. For SOFIA there will be the added constraints imposed by the limited sky visibility determined by aircraft heading. Also, sensitive observations requiring the driest conditions need to be scheduled for the highest possible aircraft altitudes. After takeoff, the initial aircraft cruising altitude is 11.6–11.9 km (38,000–39,000 ft). As fuel is burned off, the aircraft can fly higher. The performance of the aircraft allows for 6 hr of observing time above 12.5 km (41,000 ft) of which 4 hr can be above 13.1 km (43,000 ft). The maximum flight time under routine operations is 10 hr.

The flight planning process involves selecting suitable targets from a larger pool that satisfy requirements such as correct azimuth, necessary altitude, and instrument configurations. To ensure efficient use of observing time, the SOFIA Flight Planning team needs to have available a pool of targets well distributed on the sky. Figure 4 illustrates a typical flight plan from the FORCAST Basic Science period. The flight begins in Palmdale and the plan includes a mixture of galactic and extragalactic targets as well as northern and southern targets. The requirement to return to Palmdale combined with a nominal 10 hr flight length implies a maximum leg length of approximately 4 hr on a given source.

Figure 4.

Figure 4. Representative SOFIA flight plan for the FORCAST Basic Science period. Targets came from the pool of selected GI proposals. Total flight duration for this plan is 9.5 hr.

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During the 11 months of Early Science, SOFIA conducted 30 observational flights with more than 200 hr of research time. SOFIA is planned to ultimately fly approximately 120 flights per year with more than 960 research hours.

5. ACCESSING EARLY SCIENCE DATA FROM THE SOFIA ARCHIVE

Data accumulated during all flights are archived in the SOFIA data archive. The raw data (Level 1) obtained during science flights are ingested into the archive and made available for download to the program GI within 24 hr. These data are available in standard FITS format, with header information and appropriate Flexible Image Transport System (FITS) keywords conforming to the SOFIA FITS keyword dictionary. Raw FORCAST data must be corrected for several instrumental effects, including response nonlinearity, field distortion, and image artifacts. SOFIA mission operations are responsible for this processing of the FORCAST data via a software pipeline. These Level 2 data (corrected for instrumental and atmospheric effects) are scientifically valid and available for download from the SOFIA archive within two weeks after the completion of the flight series in which they are taken.

As a Principal Investigator class instrument, the GREAT data follow a somewhat different path. The raw data are archived in the SOFIA data archive, but the instrument team provides support for the subsequent processing of the data into scientifically useful products.

Nominally, data are accessible to the general community after a proprietary period of 12 months, starting from the time of ingestion into the archive. However, FORCAST Early Science data, including those presented in this volume, have a limited proprietary period and are now available to the community. Readers wishing to download FORCAST Early Science data must register an account with the SOFIA Data Cycle System (DCS), linked to and accessible from the SOFIA World Wide Web home page (https://dcs.sofia.usra.edu).

6. CONCLUDING REMARKS

SOFIA has completed over 30 science flights in the year since the initial Early Science flight in 2010 December. Some of the results of the first four flights with FORCAST are presented here in this issue, with many more results from Early Science in preparation. Another set of papers based on GREAT observations is being published in parallel in Astronomy and Astrophysics. With the range of current and future instrumentation, and with the projected 20 year operational lifetime, it is expected that SOFIA observations will yield a rich collection of scientific results of which these are the preview.

SOFIA science mission operations are conducted jointly by the Universities Space Research Association, Inc. (USRA), under NASA contract NAS2-97001, and the Deutsches SOFIA Institut (DSI) under DLR contract 50 OK 0901 to the University of Stuttgart. R.D.G. was supported by NASA and the United States Air Force.

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10.1088/2041-8205/749/2/L17